From Handwiki - Reading time: 2 minA three-dimensional model of 382 Dodona based on its light curve | |
| Discovery | |
|---|---|
| Discovered by | Auguste Charlois |
| Discovery date | 29 January 1894 |
| Designations | |
| (382) Dodona | |
| Pronunciation | /dəˈdoʊnə/[1] |
| Named after | Dodona |
| 1894 AT | |
| Minor planet category | Main belt |
| Orbital characteristics[2] | |
| Epoch 31 July 2016 (JD 2457600.5) | |
| Uncertainty parameter 0 | |
| Observation arc | 122.21 yr (44636 d) |
| |{{{apsis}}}|helion}} | 3.6577 astronomical unit|AU (547.18 Gm) |
| |{{{apsis}}}|helion}} | 2.58301 AU (386.413 Gm) |
| 3.1204 AU (466.81 Gm) | |
| Eccentricity | 0.17221 |
| Orbital period | 5.51 yr (2013.3 d) |
| Mean anomaly | 6.32892° |
| Mean motion | 0° 10m 43.716s / day |
| Inclination | 7.3928° |
| Longitude of ascending node | 313.511° |
| 270.036° | |
| Physical characteristics | |
| Dimensions | 58.37±2.8 km[2] 58.37 km[3] |
| Rotation period | 4.113 h (0.1714 d) |
| Geometric albedo | 0.1610±0.017[2] 0.161[3] |
| M | |
| Absolute magnitude (H) | 8.77[2][3] |
Dodona (minor planet designation: 382 Dodona) is a large Main belt asteroid that was discovered by the French astronomer Auguste Charlois on 29 January 1894 in Nice. It is classified as an M-type asteroid.
Measurements of the thermal inertia of 115 Thyra give an estimated range of 15–150 J m−2 K−1 s−1/2, compared to 50 for lunar regolith and 400 for coarse sand in an atmosphere.[3]